Abstract
Mössbauer spectra from intermediate pyrrhotite (Fe1-xS) samples were interpreted according to their hyperfine magnetic field distribution functions at the Fe nuclei in these sulfides. Seven non-equivalent Mössbauer sites for Fe were distinguished by their peak positions in the distribution functions obtained.
Original language | English |
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Pages (from-to) | 423-429 |
Number of pages | 7 |
Journal | Journal of Radioanalytical and Nuclear Chemistry Letters |
Volume | 153 |
Issue number | 6 |
DOIs | |
State | Published - Apr 1991 |
Externally published | Yes |